对流层使无线电射线散焦

R. E. Wilkerson
{"title":"对流层使无线电射线散焦","authors":"R. E. Wilkerson","doi":"10.6028/JRES.066D.047","DOIUrl":null,"url":null,"abstract":"When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D\" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an \"exponential\" atmosphere (troposphere).","PeriodicalId":398550,"journal":{"name":"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation","volume":"13 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1962-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Defocusing of radio rays by the troposphere\",\"authors\":\"R. E. Wilkerson\",\"doi\":\"10.6028/JRES.066D.047\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D\\\" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an \\\"exponential\\\" atmosphere (troposphere).\",\"PeriodicalId\":398550,\"journal\":{\"name\":\"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation\",\"volume\":\"13 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1962-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.6028/JRES.066D.047\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Research of the National Bureau of Standards, Section D: Radio Propagation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.6028/JRES.066D.047","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

摘要

当射电射线穿过大气层时,由于大气层的存在而被驱散。这种效应用散度系数a来衡量,并推导出了在光滑球形地球条件下,直射光的散度系数D1和反射光的散度系数D的一般公式。举例来说,在“指数”大气(对流层)的一些典型情况下,给出了DI和Dz。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Defocusing of radio rays by the troposphere
When radio rays pass through t he atmosphere, they are defoc Llsed due to its presence. This effect is measu red by the divergence coefficient a nd general formulas are derived for D1, the divergence coefficient of t he direct ray, and D" the divergence coefficient of the reflected rayassuming a smooth spherical earth . As examples, DI and Dz are shown for some typical cases with an "exponential" atmosphere (troposphere).
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信